Soil microbes produce less atmospheric CO2 than expected with
climate warming
Tuesday, April 27, 2010
The physiology of microbes living underground could determine the
amount of carbon dioxide emitted from soil on a warmer Earth,
according to a study published online this week in Nature
Geoscience.
Researchers at UC Irvine, Colorado State University and the Yale
School of Forestry & Environmental Studies found that as global
temperatures increase, microbes in soil become less efficient over
time at converting carbon in soil into carbon dioxide, a key
contributor to climate warming.
Microbes, in the form of bacteria and fungi, use carbon for energy
to breathe, or respire, and to grow in size and in number. A model
developed by the researchers shows microbes exhaling carbon dioxide
furiously for a short period of time in a warmer environment,
leaving less carbon to grow on. As warmer temperatures are
maintained, the less efficient use of carbon by the microbes causes
them to decrease in number, eventually resulting in less carbon
dioxide being emitted into the atmosphere.
"Microbes aren't the destructive agents of global warming that
scientists had previously believed," said Steven Allison, assistant
professor of ecology & evolutionary biology at UCI and lead
author on the study. "Microbes function like humans: They take in
carbon-based fuel and breathe out carbon dioxide. They are the
engines that drive carbon cycling in soil. In a balanced
environment, plants store carbon in the soil and microbes use that
carbon to grow. The microbes then produce enzymes that convert soil
carbon into atmospheric carbon dioxide."
The study, "Soil-Carbon Response to Warming Dependent on Microbial
Physiology," contradicts the results of older models that assume
microbes will continue to spew ever-increasing amounts of carbon
dioxide into the atmosphere as the climate continues to warm. The
new simulations suggest that if microbial efficiency declines in a
warmer world, carbon dioxide emissions will fall back to
pre-warming levels, a pattern seen in field experiments. But if
microbes manage to adapt to the warmth – for instance, through
increased enzyme activity – emissions could intensify.
"When we developed a model based on the actual biology of soil
microbes, we found that soil carbon may not be lost to the
atmosphere as the climate warms," said Matthew Wallenstein of the
Natural Resource Ecology Laboratory at Colorado State University.
"Conventional ecosystem models that didn't include enzymes did not
make the same predictions."
Mark Bradford, assistant professor of terrestrial ecosystem ecology
at Yale, said there is intense debate in the scientific community
over whether the loss of soil carbon will contribute to global
warming. "The challenge we have in predicting this is that the
microbial processes causing this loss are poorly understood," he
said. "More research in this area will help reduce uncertainties in
climate prediction."
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University of California - Irvine
Thanks to University of California - Irvine for this
article.